000 AXPZ20 KNHC 240935 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 1005 UTC SUN JUN 24 2007 TROPICAL WEATHER DISCUSSION FOR THE EASTERN PACIFIC OCEAN FROM THE EQUATOR TO 32N...EAST OF 140W. BASED ON 0600 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 0900 UTC. ...TROPICAL WAVES... TROPICAL WAVE ALONG 97N N OF 4N TO THE COAST OF S MEXICO IS MOVING W 10-15 KT. BROAD MID LEVEL CURVATURE IS OBSERVED ON SATELLITE IMAGERY JUST N OF THE ITCZ. CLUSTERS OF SCATTERED MODERATE/STRONG CONVECTION ARE WITHIN THE ITCZ FROM 7N-11N BETWEEN 92W-99W. TROPICAL WAVE ALONG 108W FROM 3N TO 17N IS MOVING W 10-15 KT. BROAD MID LEVEL ROTATION IS OBSERVED ON SATELLITE IMAGERY WITHIN 200 NM ALONG THE WAVE AXIS CENTERED NEAR THE ITCZ. CLUSTERS OF SCATTERED MODERATE CONVECTION ARE FROM 7N-13N BETWEEN 108W-112W. TROPICAL WAVE ALONG 125W/126W FROM 3N TO 14N IS MOVING W 10-15 KT. MID LEVEL ROTATION IS OBSERVED ON SATELLITE IMAGERY JUST TO THE E OF THE WAVE AXIS NEAR 12N123.5W. SCATTERED MODERATE/ ISOLATED STRONG CONVECTION IS WITHIN 45 NM OF 13N FROM 120W-124W. CLUSTERS OF SCATTERED MODERATE CONVECTION ARE FROM 7N-11N BETWEEN 121W-126W. ..ITCZ... ITCZ AXIS IS CENTERED ALONG 9N83W 8N91W 9N100W 8N116W 7N129W 8N140W. IN ADDITION TO CONVECTION ASSOCIATED WITH TROPICAL WAVES...SCATTERED MODERATE/STRONG CONVECTION WITHIN 60/75 NM OF 100W FROM 10N TO 14N AND WITHIN 60 NM ALONG COAST OF GUATEMALA AND MEXICO BETWEEN 90W AND 91W. CLUSTERS OF SCATTERED MODERATE/ISOLATED STRONG CONVECTION ARE WITHIN 120 NM OF THE ITCZ AXIS FROM 80W-90W. ...DISCUSSION... E OF 120W... MID/UPPER TROUGH EXTENDS FROM SW TEXAS SW ACROSS NW MEXICO TO A WEAK MID/UPPER LEVEL LOW 18N118W. DIVERGENCE TO THE SE OF THE TROUGH IS AIDING ITCZ CONVECTION ASSOCIATED WITH THE TROPICAL WAVE ALONG 108W. NEAR STATIONARY UPPER LEVEL HIGH REMAINS CENTERED OVER SW MEXICO NEAR 19N103W WITH A RIDGE EXTENDING SW TO 14N110W. UPPER LEVEL HIGH LOCATED OVER THE FAR SW CARIBBEAN EXTENDS A RIDGE W INTO THE E PACIFIC REGION TO NEAR 14N99W. THE UPPER FLOW IS LIGHT TO MODERATE OVER THE PACIFIC S OF THIS RIDGE. DIVERGENCE DUE TO THE UPPER RIDGE IS ENHANCING CONVECTION ALONG THE ITCZ ALONG 100W AS WELL AS CONVECTION OVER MUCH OF CENTRAL AMERICA AND S MEXICO. W OF 120W... NEAR STATIONARY MID/UPPER LEVEL HIGH NEAR 21N127W WITH A RIDGE AXIS EXTENDING NE TO BEYOND 32N118W AND SW OUT OF THE REGION NEAR 13N140W. STRONG SUBSIDENCE AND ASSOCIATED DRY STABLE DOMINATE THIS AREA WITHIN 250 NM OF THE RIDGE AXIS THUS LIMITING CLOUDS AND SHOWERS IN THE AREA. AT THE SURFACE... BROAD SURFACE RIDGE EXTENDS FROM A 1030 MB HIGH WELL NW OF THE REGION THROUGH 32N137W TO 20N122W. BROKEN/OVERCAST STRATOCUMULUS CLOUDS MOVING SW COVER MUCH OF THE AREA W OF 110W. DIFFERENCE IN PRESSURE BETWEEN THE BROAD RIDGE OVER THE E PACIFIC AND THE LOWER PRESSURES OVER THE SW U.S. ARE CREATING A TIGHT GRADIENT OVER THE NE PORTION TO ALLOW FOR N FLOW OF 20 KT WITH SEAS IN THE 8-10 FT RANGE IN N SWELL THROUGH THE NEXT 48 HRS. $$ WALLACE